ClimateSearch

Ōnojō, Fukuoka

Japan · 102k people · 23 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high50°F (10°C)52°F (11°C)58°F (15°C)67°F (20°C)75°F (24°C)80°F (27°C)87°F (31°C)89°F (32°C)83°F (28°C)74°F (24°C)64°F (18°C)54°F (12°C)
Average low37°F (3°C)38°F (3°C)43°F (6°C)51°F (11°C)59°F (15°C)67°F (20°C)75°F (24°C)76°F (25°C)69°F (21°C)59°F (15°C)49°F (9°C)40°F (5°C)
Dew point34°F (1°C)35°F (2°C)40°F (5°C)49°F (9°C)58°F (14°C)67°F (19°C)74°F (23°C)74°F (24°C)68°F (20°C)57°F (14°C)47°F (9°C)38°F (3°C)
Rainfall2.6 in (67 mm)2.7 in (69 mm)4.3 in (108 mm)5 in (126 mm)5.4 in (138 mm)11.1 in (282 mm)11.4 in (289 mm)6.7 in (171 mm)7.2 in (183 mm)3.7 in (94 mm)3.2 in (82 mm)2.8 in (71 mm)
Rainy days9810108121299688
Snowfall1.3 in (3.2 cm)0.9 in (2.4 cm)0.2 in (0.5 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.5 in (1.3 cm)
Sunshine111 h128 h147 h159 h159 h103 h144 h191 h161 h180 h153 h130 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+2.2°F (+1.2°C)

Models range from +2.0°F (+1.1°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

18 → 48

About 2.6× as many

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.1°F (+1.2°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.8°F (+1.5°C)
  • October: +2.6°F (+1.5°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.2°F (+1.2°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.